Title: Liquid Droplet Dynamics: Variations on a Theme
1Liquid Droplet Dynamics Variations on a Theme
- Daniel M. Anderson
- Department of Mathematical Sciences
- George Mason University
- Collaborators
- S.H. Davis, Northwestern University
- M.G. Worster, University of Cambridge
- M.G. Forest, University of North Carolina
- R. Superfine, University of North Carolina
- W.W. Schultz, University of Michigan
- J. Siddique, George Mason University
- E. Barreto, George Mason University
- B. Gluckman, George Mason University/Penn. State
University
Supported by NASA (Microgravity Science), 3M
Corporation and NSF (Applied
Mathematics DMS-0306996)
2Free-Boundary Problems in Fluid Dynamics
- the location of the free surface is part of the
solution - - surface waves in oceans, lakes
wind-driven waves
3Free-Boundary Problems in Fluid Dynamics
- the location of the free surface is part of the
solution - - surface waves in oceans, lakes
canine-driven waves
wind-driven waves
4Free-Boundary Problems in Fluid Dynamics
Fluids Spreading on Solids
- free surface with moving contact lines LARGE
SCALE - floods, lava flows (gravity)
5Free-Boundary Problems in Fluid Dynamics
The Great Molasses Flood Boston, MA 1919
- From The Boston Globe, May 28, 1996
About 2 million gallons of raw molasses burst
from a storage tank at the corner of Foster and
Commercial streets about noon on January 15,
1919. The black wave of the sticky substance was
so powerful that it knocked buildings off their
foundations and killed 21 people. Newspapers
described the cleanup effort as nightmarish
6Free-Boundary Problems in Fluid Dynamics
Fluids Spreading on Solids
- free surface with moving contact lines SMALL
SCALE - micro-fluidics, nano-fluidics (surface tension)
1mm
7Outline of Talk
- Isothermal Spreading Droplet (Plain vanilla)
- Greenspan, 1978
- Non-Isothermally Spreading Droplet
- Ehrhard Davis, 1991
- Migrating Droplet
- Smith, 1995
- Evaporating Droplet
- Anderson Davis, 1995
- Freezing Droplet
- Anderson, Worster, Davis, Schultz,
1996, 2000 - Melting Droplet
- Anderson, Forest Superfine, 2001
- Imbibing Droplet, Rigid Porous Substrate
- Hocking Davis, 2000
- Imbibing Droplet, Deformable Porous Substrate
- Anderson, 2005
- Vibrating Droplet
- Vukasinovic, Smith, Glezer, James,
2003, 2004
8Spreading Droplet Isothermal
9Anatomy of a Spreading Droplet
10Spreading Droplet Full Problem
- In the liquid
- - Navier-Stokes Equations
- Free-Surface Conditions
- - Normal and tangential stress balances
- - Mass balance (kinematic condition)
-
- Conditions at the solid boundary
- - velocity normal to interface is zero
- - slip allowed in tangential velocity
- Contact-line conditions
- - contact (droplet height is zero)
- - condition on contact angle
air
liquid
solid substrate
GOAL Identify a physical regime that corresponds
to experiments and allows isolation of
important physical effects. Reduce
mathematical model accordingly.
11Thin Film Equations Original Form
12Thin Film Equations Rescaled-Dimensionless Form
13Thin Film Equations Lubrication Theory Limit
14Isothermal Spreading Droplet Lubrication Theory
Greenspan, 1978 Ehrhard Davis, 1991, 1993
Haley Miksis, 1991
- Slow flow (Re ltlt 1) and slender geometry, zero
gravity - Full problem reduces to an evolution equation
for the interface shape
Capillary number
- symmetry conditions at
- contact line conditions
where
at
Dussan V. 1979 Ehrhard Davis, 1991, 1993
15Isothermal Droplet Spreading
- large surface tension and
- Analytical formula for
- interface shape and
- contact line position
Droplet Evolution
16Spreading Droplet Non-Isothermal
17Anatomy of a Non-isothermally-Spreading Droplet
Ehrhard Davis, 1991
18Non-Isothermal Spreading Droplet Lubrication
Theory
Ehrhard Davis, 1991, 1993
- Slow flow, slender geometry, zero gravity,
temperature-dependent surface tension - Full problem reduces to an evolution equation
for the interface shape
Marangoni effects (surface tension gradients)
capillarity (surface tension)
unsteady term
Marangoni number
Biot number (interface heat transfer)
at contact line
19Non-Isothermal Spreading Droplet Results
Ehrhard Davis, 1991, 1993
- Thermocapillary forces on interface (Marangoni
effects) - drive a flow from warmer regions to colder
regions - (surface tension decreases with temperature).
- Spreading is enhanced when substrate is cooled.
- Spreading is retarded when substrate is heated.
- Experiments using paraffin oil and silicone oil
spreading - on glass confirm these predictions.
20Migrating Droplet Non-Isothermal
21Anatomy of a Migrating Droplet
Smith, 1995
22Migrating Droplet Lubrication Theory
Smith 1995
- Slow flow, slender geometry, zero gravity,
temp.-dep surface tension - Imposed temperature variation along solid
boundary - Full problem reduces to an evolution equation
for the interface shape
Marangoni effects (surface tension gradients)
capillarity (surface tension)
unsteady term
at left and right contact lines
NOT SYMMETRIC!
23Migrating Droplet Results
Smith, 1995
- Droplet placed on a non-uniformly heated
substrate - migrates towards colder temperature region
(for - sufficiently large temperature gradients).
- Steady-state solutions include motionless drops
and drops - moving at constant speed (towards cooler
regions). - Thermocapillary-driven fluid flow in the drop
distorts - the free surface, modifies the apparent
contact angle - which in turn modifies contact line speed.
24Migrating Droplet Results
Smith, 1995
COLD
HOT
video compliments of Marc Smith, 2006
25Evaporating Droplet
26Anatomy of an Evaporating Droplet
27Evaporating Droplet
- (Anderson Davis, 1994 Hocking 1995).
- Lubrication theory leads to an evolution
equation
Marangoni effects (surface tension gradients)
evaporation (mass loss)
vapor recoil
capillarity (surface tension)
Evaporation number
Marangoni number
Scaled density ratio
Nonequilibrium param.
Slip coefficient
Capillary number
28Evaporating Droplet
- Anderson Davis, 1994 Hocking 1995.
- Lubrication theory leads to an evolution
equation
boundary conditions
contact line condition
symmetry at
at
at
liquid volume is not constant in time (droplet
vanishes in finite time)
29Evaporating Droplet
- Small capillary number (large surface tension)
Anderson Davis, 1994.
where
contact line condition
global mass balance
plus initial conditions
- Competition between spreading and evaporation
- EVAPORATION EVENTUALLY WINS!
30Evaporating Droplet
- strong evaporation,
- weak spreading
- contact line position recedes
- monotonically
- contact angle increases initially
- and remains relatively constant
31Evaporating Droplet
- weak evaporation,
- strong spreading
- contact line position advances
- initially
- contact angle decreases
- monotonically and has a nearly
- constant intermediate region
32Evaporating Droplet Results
Anderson Davis, 1995
- Evaporative effects are strongest near the
contact-line - region due to largest thermal gradients
there. - Effects that increase the contact angle retard
evaporation - - thermocapillarity flow directed
toward the colder - droplet center
- - vapor recoil nonuniform pressure
(strongest at contact - line) tends to contract the
droplet - Effects that decrease the contact angle promote
evaporation - - contact line spreading
33Freezing Droplet
34Freezing Droplet
- This problem is motivated by the need to
understand crystal growth problems and
containerless processing systems such as
Czochralski growth, float-zone processing or
surface melting. - The common feature in these systems is the
presence of a tri-junction where a liquid,
its solid and a vapor phase meet at which phase
transformation occurs. - Simple Model Problem
-
- WHAT HAPPENS WHEN WE FREEZE A LIQUID
- DROPLET FROM BELOW ON A COLD SUBSTRATE?
35Experimental Investigation (Water/Ice)
Anderson, Worster Davis (1996)
Initial, motionless, water droplet at room
temperature
36Experimental Investigation (Water/Ice)
Anderson, Worster Davis (1996)
Initial, motionless, water droplet at room
temperature
Cool bottom boundary (ethylene glycol
anti-freeze pumped through channels in bottom
plate)
Cool bottom boundary (ethylene glycol
anti-freeze pumped through channels in bottom
plate)
?
37Experimental Investigation (Water/Ice)
Anderson, Worster Davis (1996)
Initial, motionless, water droplet at room
temperature
Cool bottom boundary (ethylene glycol
anti-freeze pumped through channels in bottom
plate)
Cool bottom boundary (ethylene glycol
anti-freeze pumped through channels in bottom
plate)
38Anatomy of a Freezing Droplet
39Freezing Droplet
- surface tension dominated liquid shape
Anderson, Worster Davis, 1996.
Mass balance
Capillarity and gravity relate
Assume the solid liquid interface is planar (1D
heat conduction from cold boundary of temperature
isothermal liquid at temperature )
Tri-junction condition (3 models)
40Freezing Droplet Constant Contact Angle Model
- Contact angle in liquid is constant
Droplet Evolution
- no inflexion points
- solid shape is independent of growth rate
41Freezing Droplet Experimental Evidence
- Solidified silicon in crucible of e-beam
evaporation system (Phil Adams, LSU, 2005)
42Freezing Droplet Fixed Contact Line Model
- The tri-junction moves tangent to the liquid
vapor interface the liqiud contact angle is free
to vary
Solidified Shapes
concave down (zero slope)
concave down (nonzero slope)
concave up (nonzero slope)
- no inflexion points
- water/ice predicted to have zero slope at top
- solid shape is independent of growth rate
43Freezing Droplet Nonzero Growth Angle Model
Satunkin et al. (1980), Sanz (1986), Sanz et al.
(1987)
- The tri-junction moves at a fixed growth angle
to the liquid vapor interface (angle
through vapor phase is )
Solidified Shapes
concave down (nonzero slope)
concave up (nonzero slope)
- no inflexion point
- all materials with nonzero growth angle have
pointed top - solid shape is independent of growth rate
44Freezing Droplet Nonzero Growth Angle
simulation
Experiment ice
45Freezing Droplet
- A two-dimensional model for the thermal field in
the solid was obtained by a boundary integral
method Schultz, Worster Anderson, 2000.
46Freezing Droplet
Schultz, Worster Anderson, 2000
Results
- both peaks and dimples
- can form at the top of
- the drop (depending
- on the growth angle
- and density ratio)
- inflexion points are also
- possible
47Melting Droplet
48Melting Droplet
- Motivated by experiments on polystyrene spheres
(1mm radius) - by D. Glick UNC Physics Ph.D. 1998 with
R. Superfine
Glick Contact Angle Data
- thermal diffusion time
- 10 25 seconds
- data collapse if time is
- scaled with
138C
99C
viscosity (varies by 3 orders of magnitude in
experiment)
surface tension (varies by 10)
ad hoc length scale, increases with temperature
49Anatomy of a Melting Droplet
50Melting Droplet Model
Anderson, Forest Superfine, 2001
- initially spherical solid
- no gravity
- surface tension dominates quasi-steady liquid
vapor interface - solid-liquid interface assumed planar
Liquid Shape Spherical
Nine Unknown Functions of Time
angles
lengths
volumes and pressure
51Melting Droplet Model
Anderson, Forest Superfine, 2001
Thermal Problem
1D thermal diffusion, planar solid-liquid
interface
Motion of Solid
Balance of forces equation of motion for solid
Mass Balance
Contact-line Dynamics
Geometry
Provides five relations between lengths, angles
and volumes
Differential-Algebraic System solved by DASSL
code Brenan, Campbell, Petzold,
1995
52Melting Droplet Dynamics
Melting Droplet (medium )
characteristic contact-line speed
measures competition between spreading
and melting
characteristic melting speed
small dynamics similar to isothermal
spreading
large dynamics deviate from isothermal
spreading
53Melting Droplet Dynamics
- contact angle relaxes faster in
- spreading/melting configuration
- results do not collapse with
- rescaling of time
- contact line is less mobile in
- spreading/melting configuration
- spreading promotes melting
54Melting and Freezing Droplet
55Melting and Freezing Droplet Dynamics
56Imbibing Droplet Rigid Porous Substrate
57Anatomy of a Droplet Imbibing into a Rigid Porous
Substrate
Hocking Davis, 1999, 2000
58Imbibing Droplet Rigid Porous Substrate
Hocking Davis, 1999, 2000
- slender limit (lubrication theory)
- imbibition is one-dimensional liquid
penetrates vertically - only no radial capillarity. The porous
base is assumed to - be made up of vertical pores.
Evolution equations for liquid shape and
penetration depth
1D capillary suction flow
porosity suction parameter
porous-base modified slip coefficient
59Imbibing Droplet Rigid Porous Substrate
Hocking Davis, 1999, 2000
central region solution
Contact angle cannot be written as a
single-valued function of the contact line speed
in contrast to regular spreading.
60Imbibing Droplet Deformable Porous Substrate
61Imbibing Droplet Deformable Porous Substrate
- Motivation and Applications
- - swelling of paper/print film in inkjet
printing - - soil science
- - infiltration
- - medical science (flows in soft tissue)
Modeling Assumptions
- adopt the simplest description of fluid drop
(Hocking Davis, 2000) - assume 1D
imbibition and 1D substrate deformation
(Preziosi et al. 1996, Barry Aldis, 1992,1993)
- porous material is initially dry with uniform
solid fraction - no gravity
62Anatomy of a Droplet Imbibing into a Deformable
Substrate
63Imbibing Droplet Deformable Porous Substrate
Equations in wet/deforming porous material
Preziosi et al. 1996
solid fraction
mass conservation for solid and liquid
liquid velocity
solid velocity
modified Darcy Eq.
liquid pressure
stress equilibrium
combine into single PDE for solid fraction
permeability
solid stress
liquid viscosity
related to boundary values of solid fraction
64Imbibing Droplet Deformable Porous Substrate
Boundary Conditions
Interior similarity solution
Exterior numerical solution
65Imbibing Droplet Deformable Porous Substrate
Hocking Davis model for liquid droplet
66Deformable Substrate Sponge Problem
water dropped onto an initially dry and
compressed sponge (photos by E. Barreto and B.
Gluckman)
67Deformable Substrate 1D Sponge Problem With
Gravity
Capillary-rise of a liquid into a deformable
porous material. -- How does this compare to
the case of a rigid porous material? -- Does
the liquid rise to an equilibrium height? --
How much deformation occurs?
Ask Javed!!
68Vibrating Droplet
69Vibrating Droplet Droplet Atomization
James, Vukasinovic, Smith, Glezer (J. Fluid
Mech. 476, 2003) Vukasinovic, Smith, Glezer
(Phys. Fluids, 16, 2004)
videos compliments of Marc Smith, 2006
From JVSG During droplet ejection, the
effective mass of the dropdiaphragm system
decreases and the resonant frequency increases.
If the initial forcing frequency is above the
resonant frequency of the system, droplet
ejection causes the system to move closer to
resonance, which in turn causes more vigorous
vibration and faster droplet ejection. This
ultimately leads to drop bursting.
70Other Droplet Work
- Isothermal Spreading
- Hocking, 1992 de Gennes, 1985 Dussan V.
Davis, 1974 - Shikhmurzaev, 1997 Thompson Robbins,
1989 Koplik - Banavar, 1995 Bertozzi et al. 1998,
Barenblatt et al. 1997, - Jacqmin, 2000
- Evaporating Drops
- Hocking, 1995 Morris, 1997, 2003, 2004
Ajaev, 2005 - Freezing Drops
- Ajaev Davis, 2003
- Reactive Spreading
- Braun et al., 1995 Warren, Boettinger
Roosen, 1998 - Motion and Arrest of a Molten Droplet
- Schiaffino Sonin, 1997
- Evaporating and Migrating Droplet
- Huntley Smith, 1996
- Spreading of Hanging Droplets
- Ehrhard, 1994
AND MANY OTHERS!!!
71Summary
- The plain vanilla droplet spreading problem
and its - multiple variations lead to interesting
scientific, - experimental, mathematical modeling and
computational - problems in the general class of free-boundary
problems - in fluid mechanics and materials science.
- There are lots of variations still to explore!
72The End
- This work has been supported by
- - National Aeronautics and Space
Administration (NASA) - Microgravity Science and Application
Program - - 3M Corporation
- - National Science Foundation
- (Applied Mathematics Program,
DMS-0306996)